Abstract
In the Colorado Front Range (USA), disturbance history dictates stream planform. Undisturbed, old-growth streams have multiple channels and large amounts of wood and depositional habitat. Disturbed streams (wildfires and logging < 200 years ago) are single-channeled with mostly erosional habitat. We tested how these opposing stream states influenced organic matter, benthic macroinvertebrate secondary production, emerging aquatic insect flux, and riparian spider biomass. Organic matter and macroinvertebrate production did not differ among sites per unit area (m−2), but values were 2 ×–21 × higher in undisturbed reaches per unit of stream valley (m−1 valley) because total stream area was higher in undisturbed reaches. Insect emergence was similar among streams at the per unit area and per unit of stream valley. However, rescaling insect emergence to per meter of stream bank showed that the emerging insect biomass reaching the stream bank was lower in undisturbed sites because multi-channel reaches had 3 × more stream bank than single-channel reaches. Riparian spider biomass followed the same pattern as emerging aquatic insects, and we attribute this to bottom-up limitation caused by the multi-channeled undisturbed sites diluting prey quantity (emerging insects) reaching the stream bank (riparian spider habitat). These results show that historic landscape disturbances continue to influence stream and riparian communities in the Colorado Front Range. However, these legacy effects are only weakly influencing habitat-specific function and instead are primarily influencing stream–riparian community productivity by dictating both stream planform (total stream area, total stream bank length) and the proportional distribution of specific habitat types (pools vs riffles).
| Original language | English |
|---|---|
| Pages (from-to) | 167-180 |
| Number of pages | 14 |
| Journal | Oecologia |
| Volume | 187 |
| Issue number | 1 |
| DOIs | |
| State | Published - May 1 2018 |
Funding
Acknowledgements Funding for this project was provided by the National Science Foundation (DEB 1145616 and DEB-1146283). We are grateful to the personnel at Rocky Mountain National Park and Arapaho-Roosevelt National Forest for providing access to sampling sites. Particular thanks goes out to P. McLaughlin, M. Pita, and S. Greenley for assisting with permits. Thanks to M. Ford, E. Bays, A. Brown, T. Hammans, A. Whelan, E. Pettigrew, N. Day, R. Harrington, A. Herdrich, P. Leipzig-Scott, H. Madinger, A. McMahon, D. Slusher, E. Spiess, J. Wyer, J. Pomeranz, L. Wambolt and O. Smith for assistance in the field and laboratory. M, Kendrick, L. M. Demi, D. Nelson, and R. Zuellig assisted with analyses. Comments from the Editor in Chief of Oecologia (Joel Trexler) and two anonymous reviewers greatly improved this manuscript. This article does not contain any studies with human participants or vertebrate animals performed by any of the authors. This research was subjected to USGS review and approved for publication. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the US Government.
| Funder number |
|---|
| DEB 1145616, DEB-1146283 |
Keywords
- Disturbance
- Ecosystem size
- Fluvial geomorphology
- Legacy effect
- Subsidy
Fingerprint
Dive into the research topics of 'Shifting stream planform state decreases stream productivity yet increases riparian animal production'. Together they form a unique fingerprint.Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver